• 한국지구과학회지
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• 제26권7호
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• pp.698-705
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• 2005

한반도 집중호우를 유발시키는 중규모대류복합체는 매우 복잡한 특성을 띠고 있다. 2004년 7월 14일 발생한 중 규모 대류복합체의 발달메커니즘을 분석한 결과, a) 대류복합체 생성 전에 강한 남서기류의 유입이 있었으며, b) 600hPa고도에서 강한 역전층이 나타났다. 역전층은 상층과 하층간의 상당온위의 차이를 유발하여 대기불안정을 더욱 강화시켰다. 그리고 c) 일반적인 중규모대류복합체 특징인 풍향의 쉬어보다는 풍속의 쉬어에 의해 대류계의 열역학 불안정이 강화되었다. 그리고 d) 흑산도 등 해안지방에 의해 유발되는 난류 및 대기불안정으로 인하여 중규모 대류복합체가 해안지방에서 발달한 것으로 보인다. 그러므로 지형에 의한 중규모 대류 복합체의 발달메커니즘 규명이 필요하다.

• 한국추진공학회지
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• 제15권2호
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• pp.68-73
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• 2011

소형위성발사체 (KSLV-I)의 발사 준비에는 다양한 규격의 질소 가스 및 초저온 액체 질소가 소요된다. 발사대 질소 공급 시스템은 고압의 질소 가스 생성, 추진제 충전 후 발사 대기 중인 발사체의 보호를 위한 공간 퍼지용 질소 가스 생성, 연료 및 산화제의 냉각을 위한 액체 질소 공급 기능을 수행하기 위하여 개발되었다. 대기 환경 조건에 따라 열전달 특성이 민감하게 변화하는 대기식 기화기의 운용 불안정성을 제거하기 위해 기화기의 병렬 설치 및 교대 운용 절차를 도입하였다. 이를 통하여 기후 조건에 상관없이 항시적으로 운용이 가능한 시스템을 개발하였으며, 소형 위성 발사체의 비행 시험을 위한 발사대 운용을 성공적으로 수행하였다.

• 한국연소학회:학술대회논문집
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• 대한연소학회 2003년도 제27회 KOSCO SYMPOSIUM 논문집
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• pp.103-108
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• 2003

The effect of equivalence ratio and fuel/air mixing quality on the phase-resolved gas temperatures at different phases of the oscillating pressure cycle was experimentally investigated. An atmospheric pressure, optically accessible and laboratory-scale dump combustor operating on methane with heat release rate of 1.59kW was used. Temperature measurements were made using coherent anti-Stokes Raman spectroscopy (CARS) at several spatial locations for typical unstable combustion conditions. Analysis was conducted using parameters such as phase-resolved averaged temperature, normalized standard deviation and temperature probability distribution functions (PDFs). Also the probability on the occurrence of high temperature (over 1900K) was investigated to get the information on the perturbation of equivalence ratio and NOx emission characteristics. It was shown that most of temperature histograms exhibit Gaussian profile which has short breadth of temperature fluctuation at equivalence ratio of 0.6, while beta profile was predominant for the cases of other equivalence ratios (${\Phi}$=0.55, 0.50). The characteristics on the occurrence of high temperature also displayed periodic wave form which is very similar to the pressure signal. And the amplitude of this profile goes larger as the fuel/air mixing quality become poorer. These also provided additional information on the perturbation of equivalence ratio at flame as well as NOx emission characteristics.

• Journal of the korean society of oceanography
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• 제32권3호
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• pp.93-102
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• 1997

Coastal circulations during the (surface condition of an) idealized cold-air outbreak are numerically investigated with two-dimensional, non-hydrostatic model in which a constant bottom-slope exists. The atmospheric forcing during a cold-air outbreak is incorporated as the surface cooling and the wind stress. When the offshore angle of the wind-stress vector, defined as the angle measured from the alongshore axis, is smaller than 45 degrees, a strong downwelling circulation develops near the coast. A sharp density front, which separates the vertically homogeneous region from the offshore stratified region, is formed near the coast and propagates offshore with time. Onshore side of the density front, small-scale circulation cells which are aligned in the direction perpendicular to the bottom begin to develop as the near-coast homogeneous region broadens. The surface cooling enhances greatly the development of the surface mixed layer by convective motions due to hydrostatic instability. The convective motions reach far below the hydrostatically unstable layer which is attached to the surface. The small-scale circulation cells are appreciably modified by the convetion cell and the density front develops far offshore compared to the case of no surface cooling. As to the effect of the bottom slope, the offshore distance of the density front increases (decreases) as the bottom slope decreases (increases), which results from the fact that the onshore volume-transport (Ekman transport) of the low-density upper seawater remains almost constant when the wind-stress is maintained constant. It is shown that the bottom slope is an essential factor for the formation of both the density front and the alongshore current when the surface cooling is the only forcing.

• 대한기계학회논문집A
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• 제35권11호
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• pp.1377-1382
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• 2011

최근, 화석연료의 고갈과 환경오염의 문제로 인해 차세대 신재생 에너지에 대한 관심이 증대되고 있다. 그 중 수소연료는 친환경, 저장의 용이, 손쉬운 제조 등과 같은 장점에 반해 가연범위가 넓고, 폭발의 위험성이 단점으로 대두되고 있다. 본 연구에서는 간편한 SP 시험법을 이용하여 고압수소가스 분위기 하에서 in-situ 수소취화거동을 평가할 수 있는 시험기법을 확립하고자 한다. 그 적용성을 평가하기 위해서 수소저장용기 재료로 사용되는 스테인리스강(SUS316L)을 사용하여 대기압, 고압 헬륨 및 수소가스 분위기에서 시험하였다. 실험결과, 고압 수소가스 분위기에서는 수소 침투로 인해, 대기압 및 헬륨가스 분위기하에서와 달리, 시험편 표면에 미세균열 발생과 하중-변위 선도상 소성불안정 변형 영역에서 연신율 감소를 가져왔고, 파면관찰 결과 수소취화 균열이 관찰되어 SP시험법의 유효성을 나타내었다.

• 한국추진공학회:학술대회논문집
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• 한국추진공학회 2010년도 제35회 추계학술대회논문집
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• pp.752-757
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• 2010

소형위성발사체 (KSLV-I)의 발사 준비에는 다양한 규격의 질소 가스 및 초저온 액체 질소가 소요된다. 발사대 질소 공급 시스템은 고압의 질소 가스 생성, 추진제 충전 후 발사 대기 중인 발사체의 보호를 위한 공간 퍼지용 질소 가스 생성, 연료 및 산화제의 냉각을 위한 액체 질소 공급 기능을 수행하기 위하여 개발되었다. 대기 환경 조건에 따라 열전달 특성이 민감하게 변화하는 대기식 기화기의 운용 불안정성을 제거하기 위해 기화기의 병렬 설치 및 교대 운용 절차를 도입하였다. 이를 통하여 기후조건에 상관없이 항시적으로 운용이 가능한 시스템을 개발하였으며, 소형 위성 발사체의 비행 시험을 위한 발사대 운용을 성공적으로 수행하였다.

• 대기
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• 제31권5호
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• pp.489-510
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• 2021

In this paper, we propose an algorithm for detecting convective initiation (CI) using GEO-KOMPSAT-2A/advanced meteorological imager data. The algorithm identifies clouds that are likely to grow into convective clouds with radar reflectivity greater than 35 dBZ within the next two hours. This algorithm is developed using statistical and qualitative analysis of cloud characteristics, such as atmospheric instability, cloud top height, and phase, for convective clouds that occurred on the Korean Peninsula from June to September 2019. The CI algorithm consists of four steps: 1) convective cloud mask, 2) cloud object clustering and tracking, 3) interest field tests, and 4) post-processing tests to remove non-convective objects. Validation, performed using 14 CI events that occurred in the summer of 2020 in Korean Peninsula, shows a total probability of detection of 0.89, false-alarm ratio of 0.46, and mean lead-time of 39 minutes. This algorithm can be useful warnings of rapidly developing convective clouds in future by providing information about CI that is otherwise difficult to predict from radar or a numerical prediction model. This CI information will be provided in short-term forecasts to help predict severe weather events such as localized torrential rainfall and hail.

• 한국지구과학회지
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• 제44권2호
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• pp.119-134
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• 2023

본 연구는 2021년 3월 1일부터 2일까지 영동지역에 강설이 발생했던 사례의 종관적, 열역학적, 역학적 특성을 분석한 것이다. 분석에 사용한 자료는 AWS 관측자료, 지상일기도, ERA5 재분석 자료, 레윈존데, 천리안 2A 위성 자료, WISSDOM 자료 등이다. 사례 기간 영동지역 4개소에서 관측된 적설은 10 cm 이상으로 나타났으며, 북강릉(37.4 cm)에서는 가장 많은 적설을 보였다. 종관 분석결과, 동해상 및 영동지역 주변으로 중·상층 대기의 매우 차고 건조한 대기와 상대적으로 따뜻한 하층 대기의 온도 차이로 대류 불안정이 형성되어 북강릉 지역으로 대류운의 발달과 함께 강설이 나타났다. 특히 열역학적 및 운동학적 연직 분석에서, 하층에서 온위의 연직 경도에 의한 강한 바람과 한랭이류에 의한 대류 불안정이 영동지역의 강설 발생에 큰 역할을 한 것으로 판단된다. 이러한 결과는 레윈존데의 연직 분석에서도 확인할 수 있었다.

• 대기
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• 제23권2호
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• pp.187-204
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• 2013

This study analyzed the synoptic distribution and vertical structure about four cases of precipitation occurrences using NCEP/NCAR reanalysis data and upper level data of winter intensive observation to be performed by National Institute of Meteorological Research at Bukgangneung, Incheon, Boseong during 63days from 4 JAN to 6 MAR in 2012, and Observing System Experiment (OSE) using 3DVAR-WRF system was conducted to examine the precipitation predictability of upper level data at western and southern coastal regions. The synoptic characteristics of selected precipitation occurrences were investigated as causes for 1) rainfall events with effect of moisture convergence owing to low pressure passing through south sea on 19 JAN, 2) snowfall events due to moisture inflowing from yellow sea with propagation of Siberian high pressure after low pressure passage over middle northern region on 31 JAN, 3) rainfall event with effect of weak pressure trough in west low and east high pressure system on 25 FEB, 4) rainfall event due to moisture inflow according to low pressures over Bohai bay and south eastern sea on 5 MAR. However, it is identified that vertical structure of atmosphere had different characteristics with heavy rainfall system in summer. Firstly, depth of convection was narrow due to absence of moisture convergence and strong ascending air current in middle layer. Secondly, warm air advection by veering wind with height only existed in low layer. Thirdly, unstable layer was limited in the narrow depth due to low surface temperature although it formed, and also values of instability indices were not high. Fourthly, total water vapor amounts containing into atmosphere was small due to low temperature distribution so that precipitable water vapor could be little amounts. As result of OSE conducting with upper level data of Incheon and Boseong station, 12 hours accumulated precipitation distributions of control experiment and experiments with additional upper level data were similar with ones of observation data at 610 stations. Although Equitable Threat Scores (ETS) were different according to cases and thresholds, it was verified positive influence of upper level data for precipitation predictability as resulting with high improvement rates of 33.3% in experiment with upper level data of Incheon (INC_EXP), 85.7% in experiment with upper level data of Boseong (BOS_EXP), and 142.9% in experiment with upper level data of both Incheon and Boseong (INC_BOS_EXP) about accumulated precipitation more than 5 mm / 12 hours on 31 January 2012.

• Wind and Structures
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• 제10권4호
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• pp.367-382
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• 2007

A nonlinear numerical method was developed to assess the stability of suspension bridge catwalks under a wind load. A section model wind tunnel test was used to obtain a catwalk's aerostatic coefficients, from which the displacement-dependent wind loads were subsequently derived. The stability of a suspension bridge catwalk was analyzed on the basis of the geometric nonlinear behavior of the structure. In addition, a full model test was conducted on the catwalk, which spanned 960 m. A comparison of the displacement values between the test and the numerical simulation shows that a numerical method based on a section model test can be used to effectively and accurately evaluate the stability of a catwalk. A case study features the stability of the catwalk of the Runyang Yangtze suspension bridge, the main span of which is 1490 m. Wind can generally attack the structure from any direction. Whenever the wind comes at a yaw angle, there are six wind load components that act on the catwalk. If the yaw angle is equal to zero, the wind is normal to the catwalk (called normal wind) and the six load components are reduced to three components. Three aerostatic coefficients of the catwalk can be obtained through a section model test with traditional test equipment. However, six aerostatic coefficients of the catwalk must be acquired with the aid of special section model test equipment. A nonlinear numerical method was used study the stability of a catwalk under a yaw wind, while taking into account the six components of the displacement-dependent wind load and the geometric nonlinearity of the catwalk. The results show that when wind attacks with a slight yaw angle, the critical velocity that induces static instability of the catwalk may be lower than the critical velocity of normal wind. However, as the yaw angle of the wind becomes larger, the critical velocity increases. In the atmospheric boundary layer, the wind is turbulent and the velocity history is a random time history. The effects of turbulent wind on the stability of a catwalk are also assessed. The wind velocity fields are regarded as stationary Gaussian stochastic processes, which can be simulated by a spectral representation method. A nonlinear finite-element model set forepart and the Newmark integration method was used to calculate the wind-induced buffeting responses. The results confirm that the turbulent character of wind has little influence on the stability of the catwalk.